Creep of Ice under Low Stress
Uniaxial compressive creep tests on fine-grained polycrystalline ice indicate that secondary strain-rate is proportional to σ 1.8 , where σ is applied stress, for the range 0.1 < σ < 0.5 kgf/cm 2 (10 < σ < 50 kN/m 2 ). On the basis of the present tests, earlier results su...
| Published in: | Journal of Glaciology |
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| Main Authors: | , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Cambridge University Press (CUP)
1969
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.1017/s0022143000020815 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000020815 |
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crcambridgeupr:10.1017/s0022143000020815 |
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openpolar |
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crcambridgeupr:10.1017/s0022143000020815 2024-09-15T18:15:37+00:00 Creep of Ice under Low Stress Mellor, Malcolm Testa, Richard 1969 http://dx.doi.org/10.1017/s0022143000020815 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000020815 en eng Cambridge University Press (CUP) Journal of Glaciology volume 8, issue 52, page 147-152 ISSN 0022-1430 1727-5652 journal-article 1969 crcambridgeupr https://doi.org/10.1017/s0022143000020815 2024-07-24T04:03:23Z Uniaxial compressive creep tests on fine-grained polycrystalline ice indicate that secondary strain-rate is proportional to σ 1.8 , where σ is applied stress, for the range 0.1 < σ < 0.5 kgf/cm 2 (10 < σ < 50 kN/m 2 ). On the basis of the present tests, earlier results suggesting linear viscous behaviour at low stress are believed to be invalid. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 8 52 147 152 |
| institution |
Open Polar |
| collection |
Cambridge University Press |
| op_collection_id |
crcambridgeupr |
| language |
English |
| description |
Uniaxial compressive creep tests on fine-grained polycrystalline ice indicate that secondary strain-rate is proportional to σ 1.8 , where σ is applied stress, for the range 0.1 < σ < 0.5 kgf/cm 2 (10 < σ < 50 kN/m 2 ). On the basis of the present tests, earlier results suggesting linear viscous behaviour at low stress are believed to be invalid. |
| format |
Article in Journal/Newspaper |
| author |
Mellor, Malcolm Testa, Richard |
| spellingShingle |
Mellor, Malcolm Testa, Richard Creep of Ice under Low Stress |
| author_facet |
Mellor, Malcolm Testa, Richard |
| author_sort |
Mellor, Malcolm |
| title |
Creep of Ice under Low Stress |
| title_short |
Creep of Ice under Low Stress |
| title_full |
Creep of Ice under Low Stress |
| title_fullStr |
Creep of Ice under Low Stress |
| title_full_unstemmed |
Creep of Ice under Low Stress |
| title_sort |
creep of ice under low stress |
| publisher |
Cambridge University Press (CUP) |
| publishDate |
1969 |
| url |
http://dx.doi.org/10.1017/s0022143000020815 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000020815 |
| genre |
Journal of Glaciology |
| genre_facet |
Journal of Glaciology |
| op_source |
Journal of Glaciology volume 8, issue 52, page 147-152 ISSN 0022-1430 1727-5652 |
| op_doi |
https://doi.org/10.1017/s0022143000020815 |
| container_title |
Journal of Glaciology |
| container_volume |
8 |
| container_issue |
52 |
| container_start_page |
147 |
| op_container_end_page |
152 |
| _version_ |
1810453482315972608 |